Impact of cloud microphysics and cumulus parameterization on simulation of heavy rainfall event during 7-9 October 2007 over Bangladesh

被引：19

作者：

Mahbub Alam M. ^{[1
,2
]}

机构：

[1] Theoretical Division, SAARC Meteorological Research Centre (SMRC), Dhaka

[2] Department of Physics, Khulna University of Engineering and Technology, Khulna

来源：

Journal of Earth System Science | 2014年 / 123卷 / 2期

关键词：

Cumulus parameterization; Heavy rainfall; Microphysics; WRF-ARW model;

D O I：

10.1007/s12040-013-0401-0

中图分类号：

学科分类号：

摘要：

In the present study, the Advanced Research WRF (ARW) version 3.2.1 has been used to simulate the heavy rainfall event that occurred between 7 and 9 October 2007 in the southern part of Bangladesh. Weather Research and Forecast (WRF-ARW version) modelling system with six different microphysics (MP) schemes and two different cumulus parameterization (CP) schemes in a nested configuration was chosen for simulating the event. The model domains consist of outer and inner domains having 9 and 3 km horizontal resolution, respectively with 28 vertical sigma levels. The impacts of cloud microphysical processes by means of precipitation, wind and reflectivity, kinematic and thermodynamic characteristics of the event have been studied. Sensitivity experiments have been conducted with the WRF model to test the impact of microphysical and cumulus parameterization schemes in capturing the extreme weather event. NCEP FNL data were used for the initial and boundary condition. The model ran for 72 h using initial data at 0000 UTC of 7 October 2007. The simulated rainfall shows that WSM6-KF combination gives better results for all combinations and after that Lin-KF combination. WSM3-KF has simulated, less area average rainfall out of all MP schemes that were coupled with KF scheme. The sharp peak of relative humidity up to 300 hPa has been simulated along the vertical line where maximum updraft has been found for all MPs coupled with KF and BMJ schemes. The simulated rain water and cloud water mixing ratio were maximum at the position where the vertical velocity and reflectivity has also been maximum. The production of rain water mixing ratio depends on MP schemes as well as CP schemes. Rainfall depends on rain water mixing ratio between 950 and 500 hPa. Rain water mixing ratio above 500 hPa level has no effect on surface rain. © Indian Academy of Sciences.

引用

页码：259 / 279

页数：20

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